Double origin of hydrothermal convective flux variations in the Fossa of Vulcano (Italy)-Reference-Cited by-同舟云学术

Double origin of hydrothermal convective flux variations in the Fossa of Vulcano (Italy)

Published:2007-08-17 Issue:6 Volume:70 Page:743-751
ISSN:0258-8900
Container-title:Bulletin of Volcanology
language:en
Short-container-title:Bull Volcanol

Author:

Aubert Maurice,Diliberto Serena,Finizola Anthony,Chébli Yashmin

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/s00445-007-0165-y.pdf

Reference20 articles.

1. Aubert M (1999) Practical evaluation of steady heat discharge from dormant active volcanoes: case study of Vulcarolo fissure (Mount Etna, Italy). J Volcanol Geotherm Res 92:413–429

2. Aubert M, Alparone S (2000) Hydrothermal convective flux variation related to a seismo-tectonic crisis in the Fossa of Vulcano (Italy). CR Geosci 330:603–610

3. Capasso G, Favara R, Francofonte S, Inguaggiato S (1999) Chemical and isotopic variations in fumarolic discharge and thermal waters at Vulcano Island (Aeolian Islands, Italy) during 1996: evidence of resumed activity. J Volcanol Geotherm Res 88:167–175

4. Chiodini G, Cioni R, Marini L, Panichi C (1995) Origin of fumarolic fluids of Vulcano Island, Italy and implications for volcanic surveillance. Bull Volcanol 57:99–100

5. Chiodini G, Granieri D, Avino R, Caliro S, Costa A (2005) Carbon dioxide diffuse degassing and estimation of heat release from volcanic and hydrothermal systems. J Geophys Res 110:B08204. DOI 10.1029/2004JB003542

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